冀北承德盆地髫髻山组火山岩的时代

刘健 赵越 柳小明. 冀北承德盆地髫髻山组火山岩的时代[J]. 岩石学报, 2006, 22(11): 2617-2630.
引用本文: 刘健 赵越 柳小明. 冀北承德盆地髫髻山组火山岩的时代[J]. 岩石学报, 2006, 22(11): 2617-2630.
Age of the Tiaojishan Formation volcanics in the Chengde Basin, northern Hebei province.[J]. Acta Petrologica Sinica, 2006, 22(11): 2617-2630.
Citation: Age of the Tiaojishan Formation volcanics in the Chengde Basin, northern Hebei province.[J]. Acta Petrologica Sinica, 2006, 22(11): 2617-2630.

冀北承德盆地髫髻山组火山岩的时代

  • 基金项目:

    国家自然科学基金重点项目(40132020)和国土资源大调查项目(200013000168)资助、

Age of the Tiaojishan Formation volcanics in the Chengde Basin, northern Hebei province.

  • 随着近年来的研究进展,代表燕山期大规模火山喷发的髫髻山期(蓝旗期)火山岩的年代学数据得到迅速积累.本文在结合前人对燕山地区髫髻山期(蓝旗期)火山岩U-Pb同位素定年工作的基础上,对取自冀北承德盆地兴隆山附近髫髻山组火山岩顶、底样品的锆石进行U-Pb LA-ICP-MS定年,试图进一步限定该地区髫髻山期火山岩起始和结束的时代.承德盆地髫髻山组火山岩定年结果表明,其顶部晶屑凝灰岩时代为153±1Ma(2σ),底部粗安岩时代为156±3Ma(2σ).两者时代在误差范围内一致,说明该地区髫髻山组火山岩喷发是在短时期内完成的.燕山地区髫髻山期(蓝旗期)火山岩时代综合对比分析结果表明髫髻山组(蓝旗组)火山岩初步限定的底部年龄和顶部年龄分别为158±1Ma、153±1Ma.其形成时代在晚侏罗世.土城子组(后城组)与髫髻山组(蓝旗组)火山岩的界线年龄为153±1Ma,这是第一次获得我国中生代陆相地层界线年龄.土城子组顶部的时限确定在134±2~136±2Ma之间.其沉积时代为晚侏罗世至早白垩世.而髫髻山组火山岩之下的九龙山组的时代可能亦为晚侏罗世.区域张家口组的底部时代限定在134±2Ma.
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出版历程
收稿日期:  2006-06-09
修回日期:  2006-07-05
刊出日期:  2006-11-30

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